The Ideal Crystal Structure of Cristobalite X-I: A Bridge in SiO2 Densification
Abstract
On compression of α-cristobalite SiO2 to pressures above approximately 12 GPa, a new polymorph known as cristobalite X-I forms. The existence of cristobalite X-I has been known for several decades; however, consensus regarding its exact atomic arrangement has not yet been reached. The X-I phase constitutes an important step in the silica densification process, separating low-density tetrahedral framework phases from high-density octahedral polymorphs. It is the only nonquenchable high-density SiO2 phase, which reverts to the low-density form on decompression at ambient temperature. Recently, an experimental study proposed an octahedral model of SiO2 X-I with intrinsic structural defects involving partial Si site occupancies. In contrast, our new single-crystal synchrotron X-ray diffraction experiments have shown that the ideal structure of this phase should instead be described by a defect-free model, which does not require partial occupancies. Here, the structure of cristobalite X-I consists of octahedral chains with a 4-60°-2 zigzag chain geometry. This geometry has not been previously considered but is closely related to post-quartz, stishovite, and seifertite. In addition to the ideal, defect-free crystal structure, we also present a description of the defects that are most likely to form within the X-I phase. Density functional theory calculations support our observations, confirmingmore »
- Authors:
-
- Univ. of Hawaii at Manoa, Honolulu, HI (United States)
- SUNY Buffalo, NY (United States)
- Carnegie Inst. of Washington, Argonne, IL (United States)
- Publication Date:
- Research Org.:
- Argonne National Lab. (ANL), Argonne, IL (United States)
- Sponsoring Org.:
- USDOE National Nuclear Security Administration (NNSA); USDOE Office of Science (SC), Basic Energy Sciences (BES); National Science Foundation (NSF)
- OSTI Identifier:
- 1464807
- Grant/Contract Number:
- AC02-06CH11357; NA0002006; FC52-08NA28554; EAR1440005; NA0001974; DMR1505817; FG02-99ER45775
- Resource Type:
- Accepted Manuscript
- Journal Name:
- Journal of Physical Chemistry. C
- Additional Journal Information:
- Journal Volume: 122; Journal Issue: 30; Journal ID: ISSN 1932-7447
- Publisher:
- American Chemical Society
- Country of Publication:
- United States
- Language:
- ENGLISH
- Subject:
- 37 INORGANIC, ORGANIC, PHYSICAL, AND ANALYTICAL CHEMISTRY; chemical structure; physical and chemical processes; mathematical methods; phase transitions; crystal structure
Citation Formats
Shelton, Hannah, Bi, Tiange, Zurek, Eva, Smith, Jesse, and Dera, Przemyslaw. The Ideal Crystal Structure of Cristobalite X-I: A Bridge in SiO2 Densification. United States: N. p., 2018.
Web. doi:10.1021/acs.jpcc.8b04282.
Shelton, Hannah, Bi, Tiange, Zurek, Eva, Smith, Jesse, & Dera, Przemyslaw. The Ideal Crystal Structure of Cristobalite X-I: A Bridge in SiO2 Densification. United States. https://doi.org/10.1021/acs.jpcc.8b04282
Shelton, Hannah, Bi, Tiange, Zurek, Eva, Smith, Jesse, and Dera, Przemyslaw. Wed .
"The Ideal Crystal Structure of Cristobalite X-I: A Bridge in SiO2 Densification". United States. https://doi.org/10.1021/acs.jpcc.8b04282. https://www.osti.gov/servlets/purl/1464807.
@article{osti_1464807,
title = {The Ideal Crystal Structure of Cristobalite X-I: A Bridge in SiO2 Densification},
author = {Shelton, Hannah and Bi, Tiange and Zurek, Eva and Smith, Jesse and Dera, Przemyslaw},
abstractNote = {On compression of α-cristobalite SiO2 to pressures above approximately 12 GPa, a new polymorph known as cristobalite X-I forms. The existence of cristobalite X-I has been known for several decades; however, consensus regarding its exact atomic arrangement has not yet been reached. The X-I phase constitutes an important step in the silica densification process, separating low-density tetrahedral framework phases from high-density octahedral polymorphs. It is the only nonquenchable high-density SiO2 phase, which reverts to the low-density form on decompression at ambient temperature. Recently, an experimental study proposed an octahedral model of SiO2 X-I with intrinsic structural defects involving partial Si site occupancies. In contrast, our new single-crystal synchrotron X-ray diffraction experiments have shown that the ideal structure of this phase should instead be described by a defect-free model, which does not require partial occupancies. Here, the structure of cristobalite X-I consists of octahedral chains with a 4-60°-2 zigzag chain geometry. This geometry has not been previously considered but is closely related to post-quartz, stishovite, and seifertite. In addition to the ideal, defect-free crystal structure, we also present a description of the defects that are most likely to form within the X-I phase. Density functional theory calculations support our observations, confirming the dynamic stability of the X-I geometry and reasonably reproducing the pressure of the phase transformation. The enthalpy of cristobalite X-I is higher than stishovite and seifertite, but X-I is favored as a high-pressure successor of cristobalite due to a unique transformation pathway. Elastic and lattice dynamical properties of the X-I phase show intermediate values between stable tetrahedral and octahedral polymorphs, confirming the bridge-role of this phase in SiO2 densification.},
doi = {10.1021/acs.jpcc.8b04282},
journal = {Journal of Physical Chemistry. C},
number = 30,
volume = 122,
place = {United States},
year = {Wed Jun 27 00:00:00 EDT 2018},
month = {Wed Jun 27 00:00:00 EDT 2018}
}
Web of Science